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Static and Dynamic Models of Formation Water in Sincor Area, Orinoco Belt, Venezuela

机译:古代堡垒,委内瑞拉,奥里诺科腰带静态和动态模型

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Sincor is a strategic association between PDVSA, Total and Statoil, committed to the production, upgrading and commercialization of extra heavy oil from an area covering over 325 Km2 in the Orinoco Belt (Figure 1). The Sincor area is composed of a series of stacked unconsolidated sand-shale reservoirs with good petrophysical properties. The depositional system can be divided in two main parts, Deltaic and Fluvial. Fluvial sands, mainly stacked braided channels, represent the bottom part of the reservoir. Deltaic sands go from distributary channel and mouth bar to point bar and crevasse splay. Drilling of vertical observation wells and a testing campaign started at the end of 1999. In well tests, anomalies in water salinity values were observed: an aquifer salinity of 2300 ppm, while some wells produced water at 15000 ppm. At that time, high values were considered measurement problems. In 2001, the first horizontal producers started to cut water with similar high values to those observed in some well tests. Since then a multidisciplinary study was launched aiming at defining and characterizing all water sources using well tests (15 vertical wells) and water production data (150 horizontal wells). This information has then been integrated with geological interpretation and reservoir characterization. In this paper a static model is developed using well test information from the area. The model explains why different ranges of water salinities were observed in the oil and water zones. This model was corroborated qualitatively with log information. Dynamic data confirmed and detailed further the initial model. An exponential decrease of water salinity is generally observed with increasing water production or water cut. This phenomenon is explained by probable water influx in the form of fingering from the low salinity aquifer continously displacing high salinity formation water. The exponential curve shape would depend on the tortuosity and length of the path between the water and the produced oil zones. Static and dynamic data are consistent and confirm our model of water production mechanism observed in the field.
机译:诚信是PDVSA,总和统计单之间的战略协会,致力于从奥林科带上超过325 km2的面积覆盖额外重油的生产,升级和商业化(图1)。诚信领域由一系列堆积的未扑相砂岩储层组成,具有良好的岩石物理学。沉积系统可分为两个主要部件,红细胞和河流。氟砂,主要是堆叠编织通道,代表储层的底部。 Deltaic Sands从分销渠道和嘴巴到点栏和裂隙杆。垂直观察井的钻井和测试活动于1999年底开始。在测试中,观察到水盐度值的异常:2300 ppm的含水层盐度,而一些井产出为15000ppm。那时,高值被认为是测量问题。 2001年,第一家水平生产商开始用与在一些井测试中观察到的人相似的高值。从那时起,旨在使用井测试(15种垂直井)和水生产数据(150水平井)定义和表征所有水源的多学科研究。然后,此信息已与地质解释和储层特征集成。在本文中,使用来自该区域的井测试信息开发了一种静态模型。该模型解释了为什么在油和水域中观察到为什么在油和水域观察到不同的水盐度。该模型与日志信息定性相关。动态数据确认和详细介绍了初始模型。随着水生产或水的含量,通常观察到水盐的指数下降。这种现象是通过咒语从低盐度含水层的形式的可能性的水流来解释,该现象是从低盐度含水层穿透高盐度形成水。指数曲线形状取决于水和生产的油区之间的路径的曲折和长度。静态和动态数据是一致的,并确认我们在现场观察到的水生产机制模型。

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